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Firing transformations of cretaceous clays used in the manufacturing of ceramic tiles

机译:在瓷砖生产中使用的白垩纪粘土的燃烧转化

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Mineralogical transformations caused by firing, of five different compositions used in the formulation of ceramic pastes have been studied. Test samples have been prepared by extrusion and fired in the range of 900--ll50deg.C. Analysis of the fired samples was carried out by optical microscopy. The presence of enstatite, gehlenite, hercynite and mullite and abundant vitreous phase showed neomineralization. A fluid texture was present in all the samples and phenocrysts occurred in the partially microcrystalline matrix. In this way, the ceramic ware was analogous to porhyritic type rocks, with quartz phenocrystals and a typical undulating liquidation, opaque minerals such as hematites and crystalloelastic quartz structures on grains of orthoclase. The samples with low carbonate contents were composed of bulky particles, predominantly of quartz and hematites, which are agglomerated in a vitreous matrix.
机译:已经研究了由烧成引起的矿物学转变,在陶瓷浆料配方中使用了五种不同的成分。测试样品是通过挤压制备的,并在900--ll50°C的范围内烧制。通过光学显微镜对烧成的样品进行分析。顽辉石,方铅矿,水英石和莫来石以及丰富的玻璃态的存在表明新矿化。在所有样品中均存在流体织构,并且在部分微晶基质中出现了隐晶。这样,该陶瓷器皿类似于多孔质型岩石,具有石英表晶体和典型的起伏状液体,不透明的矿物,如赤铁矿和原钙石晶粒上的晶体弹性石英结构。碳酸盐含量低的样品由大块的颗粒组成,主要是石英和赤铁矿,它们聚集在玻璃状基质中。

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